Mica is a silicate sheet often used for its properties in the electronics field. Mica's density is 2883 micrograms per cubic millimeter.
u will need the density. density = mass / volume so mass = volume x density
In a simple way, since density = mass /volume, the density of an object can be changed by changing either mass or volume of an object .
Density. An object will float in a substance if its density is less than the density of the substance. The density of water is 1 kg /L or 1 g/ cm3. Anything with a density less than this will float.
It's actually pretty easy. If the density of the substance is higher than the density of water, the object will sink. If the density of the substance is lower than the density of water, the object will float. Be aware though that various substances may have dissolved into the water, thus changing its density. For example, seawater has a different density than fresh water.
D=m/v Density=mass/volume de= ma/vo Density = Mass/Volume
Micas are monoclinic.
Cynthia Micas is 165 cm.
Cynthia Micas was born on February 2, 1990, in Berlin, Germany.
Your question is unclear. Muscovite is not a group name, but there are a number of polytypes, as listed by Fleischer's Glossary, 2008: -2M1, -1M, , and -2M2. The micas are divided into three main subgroups: true micas, brittle micas, and interlayer-deficient micas. These total about 44 species. There are also six incompletely investigated micas that are now considered to be series.
phyllite is a type of metasedimentary rock. The parent rock likely contained clays and/or micas, which have metamorphosed into micas and aligned due to pressure. This shiny surface is produced by the alignment of the minerals.
The silicon-oxygen tetrahedral bonds in micas create a sheet structure with weak bonds between the sheets. This allows micas to cleave along these weak planes, resulting in their characteristic perfect basal cleavage.
Platy minerals are micas(muscovite and biotite) and chlorite
The silicon-oxygen tetrahedra in micas are arranged in sheets, allowing for weak bonds between the layers. This layered structure is what gives micas their characteristic cleavage properties, as the weak bonds between the layers allow the mineral to easily split along parallel planes.
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)
Minerals could include clays, feldspars, quartz, micas, and pyrite
The 'common' or rock-forming minerals, such as quartz, feldspars, micas, calcite, etc.
The micas are used as dielectrics.